Rock Identifier
Sandstone (Sedimentary Rock (Quartzose Sandstone)) — sedimentary
sedimentary

Sandstone

Sedimentary Rock (Quartzose Sandstone)

Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None, breaks across grains.

Hardness
6-7 on Mohs scale (due to quartz grains)
Luster
Dull to earthy
Identified More sedimentary
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Physical properties

Hardness: 6-7 on Mohs scale (due to quartz grains); Color: Varies widely including tan, brown, yellow, red, grey, pink, white; Luster: Dull to earthy; Crystal structure: Clastic texture composed of sand-sized mineral particles or rock fragments; Cleavage: None, breaks across grains.

Formation & geological history

Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments (predominantly quartz) in environments such as deserts, rivers, beaches, and shallow marine areas over millions of years.

Uses & applications

Widely used in construction as building stone, dimension stone, paving material, and in the manufacturing of glass and abrasives.

Geological facts

Sandstone formations often create striking geological landmarks such as arches, canyons, and monuments due to differential weathering. Famous examples include the walls of the Grand Canyon and Petra in Jordan.

Field identification & locations

Identified in the field by its gritty texture like sandpaper and visible sand grains. Found worldwide in sedimentary basins, river valleys, and desert regions. Good indicator of ancient depositional environments.